{"pageNumber":"6150","pageRowStart":"153725","pageSize":"25","recordCount":184938,"records":[{"id":68433,"text":"ha531 - 1974 - Floods in Waiahole-Waikane area, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2023-03-07T22:27:11.375674","indexId":"ha531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"531","title":"Floods in Waiahole-Waikane area, Oahu, Hawaii","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha531","usgsCitation":"Ewart, C., and Lee, R., 1974, Floods in Waiahole-Waikane area, Oahu, Hawaii: U.S. Geological Survey Hydrologic Atlas 531, 1 Plate: 38.50 x 29.50 inches, https://doi.org/10.3133/ha531.","productDescription":"1 Plate: 38.50 x 29.50 inches","costCenters":[],"links":[{"id":413799,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15922.htm","linkFileType":{"id":5,"text":"html"}},{"id":89959,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/531/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186681,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2000","country":"United States","state":"Hawaii","otherGeospatial":"Oahu, Waiahole-Waikane area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -157.838,\n 21.458\n ],\n [\n -157.838,\n 21.521\n ],\n [\n -157.9,\n 21.521\n ],\n [\n -157.9,\n 21.45833333333332\n ],\n [\n -157.838,\n 21.458\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a54","contributors":{"authors":[{"text":"Ewart, Charles J.","contributorId":88759,"corporation":false,"usgs":true,"family":"Ewart","given":"Charles J.","affiliations":[],"preferred":false,"id":278202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, R.","contributorId":97153,"corporation":false,"usgs":true,"family":"Lee","given":"R.","affiliations":[],"preferred":false,"id":278203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15535,"text":"ofr74339 - 1974 - Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73","interactions":[],"lastModifiedDate":"2024-02-23T19:33:40.536288","indexId":"ofr74339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-339","title":"Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73","docAbstract":"

The Reedy Creek Improvement District (hereinafter called the RCID) is an area of about 43 square miles (111. square kilometres) in southwest Orange and northwest Osceola Counties. Before development of Walt Disney World began (mid-1967), all of this tract of land was scrubby flatlands and swamp. Walt Disney World facilities now (1974) occupy slightly less than 10 percent of the area. Hydrologic data are available for most of the area for the 6-year period July 1967-June 1973, with some records starting before July 1967.

The potentiometric surface of the Floridan aquifer near Bay Lake has declined 8 feet (2 metres) on the average. Seventy-five percent of the decline is attributed to water use in the RCID; the remaining decline is attributed to deficient rainfall since the records began in March 1966. The discharge of streams in the RCID has apparently increased. However, the hydrologic conditions were changing locally as the development of the area progressed. Because of this change, the magnitude and seasonal distribution of any eventual change in streamflow cannot be accurately appraised until additional data are obtained after the development has stabilized. Some changes in water quality have occurred, but none can be attributed to urbanization.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74339","collaboration":"Prepared in cooperation with the Reedy Creek Improvement District","usgsCitation":"Putnam, A.L., 1974, Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73: U.S. Geological Survey Open-File Report 74-339, ix, 129 p., https://doi.org/10.3133/ofr74339.","productDescription":"ix, 129 p.","costCenters":[],"links":[{"id":425959,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0339/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0339/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Orange County, Osceola County","otherGeospatial":"Reedy Creek Improvement District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.60730309556335,\n 28.489196384290096\n ],\n [\n -81.60730309556335,\n 28.395006686287886\n ],\n [\n -81.50978150298498,\n 28.395006686287886\n ],\n [\n -81.50978150298498,\n 28.489196384290096\n ],\n [\n -81.60730309556335,\n 28.489196384290096\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69919c","contributors":{"authors":[{"text":"Putnam, Arthur L.","contributorId":25170,"corporation":false,"usgs":true,"family":"Putnam","given":"Arthur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68593,"text":"ha522 - 1974 - Water resources of the Cannon River watershed, southeastern Minnesota","interactions":[{"subject":{"id":44062,"text":"ofr738 - 1973 - Water resources of the Cannon River watershed, southeastern Minnesota","indexId":"ofr738","publicationYear":"1973","noYear":false,"title":"Water resources of the Cannon River watershed, southeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68593,"text":"ha522 - 1974 - Water resources of the Cannon River watershed, southeastern Minnesota","indexId":"ha522","publicationYear":"1974","noYear":false,"title":"Water resources of the Cannon River watershed, southeastern Minnesota"},"id":1}],"lastModifiedDate":"2018-03-05T10:19:00","indexId":"ha522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"522","title":"Water resources of the Cannon River watershed, southeastern Minnesota","docAbstract":"

The 1,462 square miles of land surface in the Cannon River watershed varies considerably from areas of low hills and plains to areas dominated by streams deeply incised into bedrock. Much of the south-central part of the area consists of a till plain that ranges in altitude from 1,100 to 1,200 feet above mean sea level. This plain is bordered by end moraines that form ridges on the east, west, and south. The eastern moraine marks the maximum eastward extend of the Wisconsin glacier, rising to more than 1,300 feet above sea level and forming ridges 50 to 100 feet above the till plain. In the northwest, the end moraine ridges are less obvious but extend directly north across the Cannon River valley.

\n

The end moraine ridges were cut by glacial melt water, which also deepened the pre-existing Cannon River valley. This deeply incised valley captures some of the streams that flow westward off the end moraines.

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East of the end moraines, pre-Wisconsin age glacial deposits are relatively thin and deeply weathered and eroded.

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Lard glacial melt-water valleys, around Cannon Falls and extending several miles to the west and south west, are characterized by broad valley floors underlain by outwash sand and gravel. The Cannon River flows out of the watershed and enters the Mississippi River at about 660 feet altitude.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ha522","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources Division of Waters, Soils, and Minerals","usgsCitation":"Anderson, H.W., Farrell, D., Broussard, W., and Felsheim, P., 1974, Water resources of the Cannon River watershed, southeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 522, 3 Plates: 41.00 x 34.00 inches or smaller, https://doi.org/10.3133/ha522.","productDescription":"3 Plates: 41.00 x 34.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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No abstract available.

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K.","contributorId":83161,"corporation":false,"usgs":true,"family":"Armstrong","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":234380,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":59905,"text":"mf559 - 1974 - Preliminary geologic map of the Blue Basin Quadrangle, Elko County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:19","indexId":"mf559","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"559","title":"Preliminary geologic map of the Blue Basin Quadrangle, Elko County, Nevada","language":"ENGLISH","doi":"10.3133/mf559","usgsCitation":"Ketner, K.B., 1974, Preliminary geologic map of the Blue Basin Quadrangle, Elko County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 559, 1 map., https://doi.org/10.3133/mf559.","productDescription":"1 map.","costCenters":[],"links":[{"id":104177,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3663.htm","linkFileType":{"id":5,"text":"html"},"description":"3663"},{"id":182296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.11749999999999,41 ], [ -116.11749999999999,41.1175 ], [ -116,41.1175 ], [ -116,41 ], [ -116.11749999999999,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bcbf","contributors":{"authors":[{"text":"Ketner, K. B.","contributorId":23121,"corporation":false,"usgs":true,"family":"Ketner","given":"K.","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":262807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13411,"text":"ofr741024 - 1974 - Reconnaissance study of the geothermal resources of Modoc County, California","interactions":[],"lastModifiedDate":"2025-07-31T20:42:36.097194","indexId":"ofr741024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-1024","title":"Reconnaissance study of the geothermal resources of Modoc County, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741024","usgsCitation":"Duffield, W.A., and Fournier, R.O., 1974, Reconnaissance study of the geothermal resources of Modoc County, California: U.S. Geological Survey Open-File Report 74-1024, Report: i, 20 p.; 1 Plate: 20.11 x 19.23 inches, https://doi.org/10.3133/ofr741024.","productDescription":"Report: i, 20 p.; 1 Plate: 20.11 x 19.23 inches","costCenters":[],"links":[{"id":41837,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41838,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146061,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1024/report-thumb.jpg"},{"id":493288,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8845.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Modoc County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121,\n 42\n ],\n [\n -121,\n 41.175\n ],\n [\n -120,\n 41.175\n ],\n [\n -120,\n 42\n ],\n [\n -121,\n 42\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6366fd","contributors":{"authors":[{"text":"Duffield, Wendell A.","contributorId":14363,"corporation":false,"usgs":true,"family":"Duffield","given":"Wendell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":167763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fournier, Robert O.","contributorId":73202,"corporation":false,"usgs":true,"family":"Fournier","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":167764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15814,"text":"ofr74357 - 1974 - Streamflow measurement network review for hydroelectric power applications in Brazil","interactions":[],"lastModifiedDate":"2023-08-21T18:51:30.61942","indexId":"ofr74357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-357","title":"Streamflow measurement network review for hydroelectric power applications in Brazil","docAbstract":"

This review of selected segments of the stream-gaging network of Brazil was undertaken by the writer in March and April, 1973, pursuant to an agreement between Companhia de Pesquisa de Recursos Minerais (CPRM) and Centrais Eletricas Brasileiras S.A. (ELETROBRAS) as a part of the cooperative program of the U.S. Geological Survey (USGS) and CPRM under the auspices of the Ministerio das Minas e Energia (MME) and the U.S. Agency for International Development (USAID). Its primary purpose is to provide an evaluation of the adequacy of streamflow data on streams which are being considered for or are already being utilized for hydroelectric power sources. Some comments are included pertaining to the general coverage hydrologic network. These comments were generated by the examination of the streamflow data useful for power purposes because all gaging stations form a part of the total network for hydrologic investigations. Present plans are that the entire network will eventually be operated by or under the jurisdiction of the MME through the Departamento National de Aguas e Energia Eletrica (DNAEE).

Brazil is a large country, larger than the conterminous United States, and it has been engaged in hydrologic investigations for more than 50 years. The network has been maintained by Federal agencies, State agencies, power companies, and consulting firms and until recently no organizational mechanism existed to coordinate the various activities or to establish uniform standards of data collection, computation, and publication.

It is estimated that stage and/or discharge data have been collected at 2,500 or more sites in Brazil. Because there has been no centralized publication system, it has not been possible to locate with assurance all measurement sites or to ascertain precisely the types and quality of the data collected or available.

For these reasons the suggestions outlined in this report are expected to be modified on the basis of local need and site information, which may not have been evident at the time of the review. For example, specific suggestions have been made to discontinue some stations which appear superfluous or which essentially duplicate other stations. In other instances additions to the network have been proposed. There may be reasons for the continued operation of a given station which cannot be discerned from the available literature. Also coverage may have been established in an area but the evidence has not yet appeared in print. DEAEE is currently (1973) working diligently to overcome a backlog of data computation and publication. Brazil is currently developing at a rapid rate with electric power demands increasing at a 12% annually, a reflection of the tremendous growth of the economy. With this rate of increase likely to continue for the foreseable future, it goes without saying that hydrologic information needed tomorrow must be collected today.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74357","collaboration":"Prepared in cooperation with the Brazilian Ministry of Mines and Energy National Department of Water and Electrical Energy under the auspices of the United States Agency for International Development","usgsCitation":"Schaefer, F.T., 1974, Streamflow measurement network review for hydroelectric power applications in Brazil: U.S. Geological Survey Open-File Report 74-357, 63 p., https://doi.org/10.3133/ofr74357.","productDescription":"63 p.","costCenters":[],"links":[{"id":148318,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0357/report-thumb.jpg"},{"id":419982,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Brazil","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.5719146888472,\n 3.7969492210477824\n ],\n [\n -74.5719146888472,\n -33.611048620406706\n ],\n [\n -27.13000244975086,\n -33.611048620406706\n ],\n [\n -27.13000244975086,\n 3.7969492210477824\n ],\n [\n -74.5719146888472,\n 3.7969492210477824\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d89","contributors":{"authors":[{"text":"Schaefer, Francis T.","contributorId":48184,"corporation":false,"usgs":true,"family":"Schaefer","given":"Francis","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":171778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68592,"text":"ha525 - 1974 - Water resources of the Blue Earth River watershed, south-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T10:17:14","indexId":"ha525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"525","title":"Water resources of the Blue Earth River watershed, south-central Minnesota","docAbstract":"

The Blue Earth River Watershed in Minnesota includes 3,106 square miles of land surface, which varies from fairly flat to gently rolling. The drainage extends south to include an additional 450 square miles in Iowa. The western, southern, and eastern boundaries are end moraines formed by Pleistocene glaciers. Major streams have eroded channels 40 to 75 feet deep in headwater regions and 150 to 200 feet deep near the mouth of the Blue Earth River at Mankato. In their lower reaches major streams have cut through glacial deposits and into underlying bedrock (described on ground-water sheet).

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